Sea surface distribution of coccolithophores in the eastern Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas) during the late austral summer of 2001
Horizontal distributions of coccolithophores were observed in sea surface water samples collected on the RV Polarstern between 27 February and 10 April, 2001, in the Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas). These samples were analyzed to gain information about the dis...
Gespeichert in:
Veröffentlicht in: | Marine micropaleontology 2008-10, Vol.69 (1), p.16-25 |
---|---|
Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 25 |
---|---|
container_issue | 1 |
container_start_page | 16 |
container_title | Marine micropaleontology |
container_volume | 69 |
creator | Gravalosa, José M. Flores, José-Abel Sierro, Francisco J. Gersonde, Rainer |
description | Horizontal distributions of coccolithophores were observed in sea surface water samples collected on the
RV Polarstern between 27 February and 10 April, 2001, in the Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas). These samples were analyzed to gain information about the distribution of coccolithophores in relation to the oceanic fronts of the Southern Ocean. A total of fifteen species of coccolithophores were identified, showing cell abundances of up to 67
×
10
3 cells/l down to 63°S.
Emiliania huxleyi was the most abundant taxon, always accounting for more than 85% of the assemblage. The second most abundant species was
Calcidiscus leptoporus, with values lower than 7%. Cell density increases significantly in both the Subantarctic and Polar Fronts (155 and 151
×
10
3 cells/l, respectively), decreasing abruptly in the intervening Polar Frontal Zone and to the south of the Polar Front. Although temperature at high latitudes is the main factor controlling the biogeographical distribution of coccolithophores, at the regional level (Southern Ocean) the frontal systems, and consequently nutrient distribution, play a crucial role. |
doi_str_mv | 10.1016/j.marmicro.2007.11.006 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_19540528</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S037783980800042X</els_id><sourcerecordid>19540528</sourcerecordid><originalsourceid>FETCH-LOGICAL-a366t-c2f639f661b0a7112c218ccc3a6126d4fb48d0c68dd10fb09dd903087eedfa873</originalsourceid><addsrcrecordid>eNqFUU1v1DAQtRCVWFr-AvIJwSHBk2wd50ap-JIqFant2fKOx6xXib3YTiX-Er8SpwtnTqPRvPdm3jzGXoNoQYB8f2hnk2aPKbadEEML0Aohn7ENqKFrJCj5nG1EPwyN6kf1gr3M-SBEZfZyw37fkeF5Sc4gcetzSX63FB8Dj45jRIyTL_t43MdEmfvAy544mVwoBf7doHceeSYsMa2MdXoXl1rq-BbJBP72I02TDz_y3iyZAjfB8qt5CXZt6vb8jtslVcATeTKFeAWWZKZ61zzTk241BhfszJkp06u_9Zw9fP50f_21ubn98u366qYxvZSlwc7JfnRSwk6YAaDDDhQi9kZCJ-3W7bbKCpTKWhBuJ0ZrR9ELNRBZZ9TQn7M3J91jij8XykXPPmM1YQLFJWsYL7fislMVKE_A-vqcEzl9TL5m8UuD0Gs0-qD_RaPXaDSArtFU4ocTkaqNR09JZ_QUkKxP9ZXaRv8_iT9bpZ6D</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>19540528</pqid></control><display><type>article</type><title>Sea surface distribution of coccolithophores in the eastern Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas) during the late austral summer of 2001</title><source>Elsevier ScienceDirect Journals</source><creator>Gravalosa, José M. ; Flores, José-Abel ; Sierro, Francisco J. ; Gersonde, Rainer</creator><creatorcontrib>Gravalosa, José M. ; Flores, José-Abel ; Sierro, Francisco J. ; Gersonde, Rainer</creatorcontrib><description>Horizontal distributions of coccolithophores were observed in sea surface water samples collected on the
RV Polarstern between 27 February and 10 April, 2001, in the Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas). These samples were analyzed to gain information about the distribution of coccolithophores in relation to the oceanic fronts of the Southern Ocean. A total of fifteen species of coccolithophores were identified, showing cell abundances of up to 67
×
10
3 cells/l down to 63°S.
Emiliania huxleyi was the most abundant taxon, always accounting for more than 85% of the assemblage. The second most abundant species was
Calcidiscus leptoporus, with values lower than 7%. Cell density increases significantly in both the Subantarctic and Polar Fronts (155 and 151
×
10
3 cells/l, respectively), decreasing abruptly in the intervening Polar Frontal Zone and to the south of the Polar Front. Although temperature at high latitudes is the main factor controlling the biogeographical distribution of coccolithophores, at the regional level (Southern Ocean) the frontal systems, and consequently nutrient distribution, play a crucial role.</description><identifier>ISSN: 0377-8398</identifier><identifier>EISSN: 1872-6186</identifier><identifier>DOI: 10.1016/j.marmicro.2007.11.006</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Antarctic ; Calcidiscus leptoporus ; coccolithophores ; Coccolithus huxleyi ; Emiliania huxleyi ; Polar Front ; Southern Ocean ; Subantarctic Front ; Subantarctic, Pacific</subject><ispartof>Marine micropaleontology, 2008-10, Vol.69 (1), p.16-25</ispartof><rights>2008 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a366t-c2f639f661b0a7112c218ccc3a6126d4fb48d0c68dd10fb09dd903087eedfa873</citedby><cites>FETCH-LOGICAL-a366t-c2f639f661b0a7112c218ccc3a6126d4fb48d0c68dd10fb09dd903087eedfa873</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S037783980800042X$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3536,27903,27904,65309</link.rule.ids></links><search><creatorcontrib>Gravalosa, José M.</creatorcontrib><creatorcontrib>Flores, José-Abel</creatorcontrib><creatorcontrib>Sierro, Francisco J.</creatorcontrib><creatorcontrib>Gersonde, Rainer</creatorcontrib><title>Sea surface distribution of coccolithophores in the eastern Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas) during the late austral summer of 2001</title><title>Marine micropaleontology</title><description>Horizontal distributions of coccolithophores were observed in sea surface water samples collected on the
RV Polarstern between 27 February and 10 April, 2001, in the Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas). These samples were analyzed to gain information about the distribution of coccolithophores in relation to the oceanic fronts of the Southern Ocean. A total of fifteen species of coccolithophores were identified, showing cell abundances of up to 67
×
10
3 cells/l down to 63°S.
Emiliania huxleyi was the most abundant taxon, always accounting for more than 85% of the assemblage. The second most abundant species was
Calcidiscus leptoporus, with values lower than 7%. Cell density increases significantly in both the Subantarctic and Polar Fronts (155 and 151
×
10
3 cells/l, respectively), decreasing abruptly in the intervening Polar Frontal Zone and to the south of the Polar Front. Although temperature at high latitudes is the main factor controlling the biogeographical distribution of coccolithophores, at the regional level (Southern Ocean) the frontal systems, and consequently nutrient distribution, play a crucial role.</description><subject>Antarctic</subject><subject>Calcidiscus leptoporus</subject><subject>coccolithophores</subject><subject>Coccolithus huxleyi</subject><subject>Emiliania huxleyi</subject><subject>Polar Front</subject><subject>Southern Ocean</subject><subject>Subantarctic Front</subject><subject>Subantarctic, Pacific</subject><issn>0377-8398</issn><issn>1872-6186</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNqFUU1v1DAQtRCVWFr-AvIJwSHBk2wd50ap-JIqFant2fKOx6xXib3YTiX-Er8SpwtnTqPRvPdm3jzGXoNoQYB8f2hnk2aPKbadEEML0Aohn7ENqKFrJCj5nG1EPwyN6kf1gr3M-SBEZfZyw37fkeF5Sc4gcetzSX63FB8Dj45jRIyTL_t43MdEmfvAy544mVwoBf7doHceeSYsMa2MdXoXl1rq-BbJBP72I02TDz_y3iyZAjfB8qt5CXZt6vb8jtslVcATeTKFeAWWZKZ61zzTk241BhfszJkp06u_9Zw9fP50f_21ubn98u366qYxvZSlwc7JfnRSwk6YAaDDDhQi9kZCJ-3W7bbKCpTKWhBuJ0ZrR9ELNRBZZ9TQn7M3J91jij8XykXPPmM1YQLFJWsYL7fislMVKE_A-vqcEzl9TL5m8UuD0Gs0-qD_RaPXaDSArtFU4ocTkaqNR09JZ_QUkKxP9ZXaRv8_iT9bpZ6D</recordid><startdate>20081001</startdate><enddate>20081001</enddate><creator>Gravalosa, José M.</creator><creator>Flores, José-Abel</creator><creator>Sierro, Francisco J.</creator><creator>Gersonde, Rainer</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20081001</creationdate><title>Sea surface distribution of coccolithophores in the eastern Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas) during the late austral summer of 2001</title><author>Gravalosa, José M. ; Flores, José-Abel ; Sierro, Francisco J. ; Gersonde, Rainer</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a366t-c2f639f661b0a7112c218ccc3a6126d4fb48d0c68dd10fb09dd903087eedfa873</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>Antarctic</topic><topic>Calcidiscus leptoporus</topic><topic>coccolithophores</topic><topic>Coccolithus huxleyi</topic><topic>Emiliania huxleyi</topic><topic>Polar Front</topic><topic>Southern Ocean</topic><topic>Subantarctic Front</topic><topic>Subantarctic, Pacific</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gravalosa, José M.</creatorcontrib><creatorcontrib>Flores, José-Abel</creatorcontrib><creatorcontrib>Sierro, Francisco J.</creatorcontrib><creatorcontrib>Gersonde, Rainer</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Marine micropaleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gravalosa, José M.</au><au>Flores, José-Abel</au><au>Sierro, Francisco J.</au><au>Gersonde, Rainer</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Sea surface distribution of coccolithophores in the eastern Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas) during the late austral summer of 2001</atitle><jtitle>Marine micropaleontology</jtitle><date>2008-10-01</date><risdate>2008</risdate><volume>69</volume><issue>1</issue><spage>16</spage><epage>25</epage><pages>16-25</pages><issn>0377-8398</issn><eissn>1872-6186</eissn><abstract>Horizontal distributions of coccolithophores were observed in sea surface water samples collected on the
RV Polarstern between 27 February and 10 April, 2001, in the Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas). These samples were analyzed to gain information about the distribution of coccolithophores in relation to the oceanic fronts of the Southern Ocean. A total of fifteen species of coccolithophores were identified, showing cell abundances of up to 67
×
10
3 cells/l down to 63°S.
Emiliania huxleyi was the most abundant taxon, always accounting for more than 85% of the assemblage. The second most abundant species was
Calcidiscus leptoporus, with values lower than 7%. Cell density increases significantly in both the Subantarctic and Polar Fronts (155 and 151
×
10
3 cells/l, respectively), decreasing abruptly in the intervening Polar Frontal Zone and to the south of the Polar Front. Although temperature at high latitudes is the main factor controlling the biogeographical distribution of coccolithophores, at the regional level (Southern Ocean) the frontal systems, and consequently nutrient distribution, play a crucial role.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.marmicro.2007.11.006</doi><tpages>10</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0377-8398 |
ispartof | Marine micropaleontology, 2008-10, Vol.69 (1), p.16-25 |
issn | 0377-8398 1872-6186 |
language | eng |
recordid | cdi_proquest_miscellaneous_19540528 |
source | Elsevier ScienceDirect Journals |
subjects | Antarctic Calcidiscus leptoporus coccolithophores Coccolithus huxleyi Emiliania huxleyi Polar Front Southern Ocean Subantarctic Front Subantarctic, Pacific |
title | Sea surface distribution of coccolithophores in the eastern Pacific sector of the Southern Ocean (Bellingshausen and Amundsen Seas) during the late austral summer of 2001 |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-25T12%3A19%3A56IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Sea%20surface%20distribution%20of%20coccolithophores%20in%20the%20eastern%20Pacific%20sector%20of%20the%20Southern%20Ocean%20(Bellingshausen%20and%20Amundsen%20Seas)%20during%20the%20late%20austral%20summer%20of%202001&rft.jtitle=Marine%20micropaleontology&rft.au=Gravalosa,%20Jos%C3%A9%20M.&rft.date=2008-10-01&rft.volume=69&rft.issue=1&rft.spage=16&rft.epage=25&rft.pages=16-25&rft.issn=0377-8398&rft.eissn=1872-6186&rft_id=info:doi/10.1016/j.marmicro.2007.11.006&rft_dat=%3Cproquest_cross%3E19540528%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=19540528&rft_id=info:pmid/&rft_els_id=S037783980800042X&rfr_iscdi=true |